Acquisition and assimilation of nitrogen as peptide-bound and D-enantiomers of amino acids by wheat.
Acquisition and assimilation of nitrogen as peptide-bound and D-enantiomers of amino acids by wheat.
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DOI:
10.1371/journal.pone.0019220
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发表时间:
2011-04-26
期刊:
影响因子:
3.7
通讯作者:
Jones DL
中科院分区:
文献类型:
--
作者:
Hill PW;Quilliam RS;DeLuca TH;Farrar J;Farrell M;Roberts P;Newsham KK;Hopkins DW;Bardgett RD;Jones DL
Nitrogen is a key regulator of primary productivity in many terrestrial ecosystems. Historically, only inorganic N (NH4 + and NO3 -) and L-amino acids have been considered to be important to the N nutrition of terrestrial plants. However, amino acids are also present in soil as small peptides and in D-enantiomeric form. We compared the uptake and assimilation of N as free amino acid and short homopeptide in both L- and D-enantiomeric forms. Sterile roots of wheat (Triticum aestivum L.) plants were exposed to solutions containing either 14C-labelled L-alanine, D-alanine, L-trialanine or D-trialanine at a concentration likely to be found in soil solution (10 µM). Over 5 h, plants took up L-alanine, D-alanine and L-trialanine at rates of 0.9±0.3, 0.3±0.06 and 0.3±0.04 µmol g−1 root DW h−1, respectively. The rate of N uptake as L-trialanine was the same as that as L-alanine. Plants lost ca.60% of amino acid C taken up in respiration, regardless of the enantiomeric form, but more (ca.80%) of the L-trialanine C than amino acid C was respired. When supplied in solutions of mixed N form, N uptake as D-alanine was ca.5-fold faster than as NO3 -, but slower than as L-alanine, L-trialanine and NH4 +. Plants showed a limited capacity to take up D-trialanine (0.04±0.03 µmol g−1 root DW h−1), but did not appear to be able to metabolise it. We conclude that wheat is able to utilise L-peptide and D-amino acid N at rates comparable to those of N forms of acknowledged importance, namely L-amino acids and inorganic N. This is true even when solutes are supplied at realistic soil concentrations and when other forms of N are available. We suggest that it may be necessary to reconsider which forms of soil N are important in the terrestrial N cycle.
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影响因子:
6.9
作者:
Paungfoo-Lonhienne C;Schenk PM;Lonhienne TG;Brackin R;Meier S;Rentsch D;Schmidt S
通讯作者:
Schmidt S
影响因子:
3.8
作者:
Ono, Kazutoshi;Yanagida, Kazuki;Soda, Kenji
通讯作者:
Soda, Kenji
影响因子:
9.7
作者:
Jones, DL;Owen, AG;Farrar, JF
通讯作者:
Farrar, JF
影响因子:
9.7
作者:
O'Dowd, RW;Parsons, R;Hopkins, DW
通讯作者:
Hopkins, DW
影响因子:
9.7
作者:
Hill, Paul W.;Farrar, John F.;Jones, David L.
通讯作者:
Jones, David L.